2001•Geology and ProspectingRequires access

OCCURRENCE AND DISTRIBUTION OF GOLD IN THE TIANMASHAN SULFUR-GOLD DEPOSIT

Xia Yuan-f

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Abstract

Gold occurs mainly in mineral state. Only a small amount is in fine-grained dispersed phase. Gold-Carrying minerals are mainly chalcopyrite, arsenopyrite, pyrite, gangue, pyrrhotite and so on. Gold minerals are mainly Gold, silver-gold, the fineness averaging 745.57. Gold is embedded as inter-crystal, inclusion and fissure-filling form. Gold is uneven distributed in ores and orebodies. Correlation of Gold to sulfur, gold to arsenic depend on types of orebodies and ores.

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What this paper is about

Gold occurs mainly in mineral state. Only a small amount is in fine-grained dispersed phase. Gold-Carrying minerals are mainly chalcopyrite, arsenopyrite, pyrite, gangue, pyrrhotite and so on. Gold minerals are mainly Gold, silver-gold, the fineness averaging 745.57. Gold is embedded as inter-crystal, inclusion and fissure-filling form. Gold is uneven distributed in ores and orebodies. Correlation of Gold to sulfur, gold to arsenic depend on types of orebodies and ores.

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Available abstract

Gold occurs mainly in mineral state. Only a small amount is in fine-grained dispersed phase. Gold-Carrying minerals are mainly chalcopyrite, arsenopyrite, pyrite, gangue, pyrrhotite and so on. Gold minerals are mainly Gold, silver-gold, the fineness averaging 745.57. Gold is embedded as inter-crystal, inclusion and fissure-filling form. Gold is uneven distributed in ores and orebodies. Correlation of Gold to sulfur, gold to arsenic depend on types of orebodies and ores.

Key concepts: Arsenopyrite, Pyrite, Gangue, Pyrrhotite, Fineness, Gold ore, Chalcopyrite, Geology

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